内陆地震2024,Vol.38Issue(4) :340-348.DOI:10.16256/j.issn.1001-8956.2024.04.005

乌什MS7.1地震序列特征研究

STUDY ON THE CHARACTERISTICS OF THE 2024 WUSHI MS7.1 EARTHQUAKE SEQUENCE

南芳芳 向元 张锋 黄帅堂 聂晓红
内陆地震2024,Vol.38Issue(4) :340-348.DOI:10.16256/j.issn.1001-8956.2024.04.005

乌什MS7.1地震序列特征研究

STUDY ON THE CHARACTERISTICS OF THE 2024 WUSHI MS7.1 EARTHQUAKE SEQUENCE

南芳芳 1向元 2张锋 3黄帅堂 2聂晓红2
扫码查看

作者信息

  • 1. 新疆维吾尔自治区地震局阿克苏地震监测中心站,新疆阿克苏 843000
  • 2. 新疆维吾尔自治区地震局,新疆乌鲁木齐 830011
  • 3. 新疆维吾尔自治区地震局和田地震监测中心站,新疆和田 848000
  • 折叠

摘要

深入分析2024年1月23日乌什MS7.1地震序列的活动特征、序列参数以及序列类型.结果表明:乌什MS7.1地震余震序列丰富,地震活动强度衰减较为缓慢,呈起伏式衰减特征;地震频度总体衰减较快.余震主要分布在盆山交接部位,长约200 km,宽约150 km,整体呈NE向展布.4次MS>5.5强余震前一定程度表现出p值和h值偏低的现象.根据序列中最大地震的能量释放比、b值以及主震与最大余震震级的差值的情况分析,2024年1月23日乌什MS7.1地震序列类型属于主震—余震型.

Abstract

In depth analysis of the activity characteristics,sequence parameters,and sequence types of the Wushi MS7.1 earthquake sequence on January 23,2024 shows that the aftershock sequence of the Wushi MS7.1 earthquake is rich,and the intensity of seismic activity decays slowly,showing a fluctuating attenuation characteristic;The overall attenuation of earthquake frequency is relatively fast.The aftershocks are mainly distributed at the junction of the basin and mountains,with a length of about 200 km and a width of about 150 km,and are generally distributed in the NE direction.Before 4 strong aftershocks with MS>5.5,there was a certain degree of low p-values and h-values.Based on the analysis of the energy release ratio,b-value,and the difference in magnitude between the main shock and the maximum aftershock of the largest earthquake in the sequence,the Wushi Ms7.1 earthquake sequence on January 23,2024 belongs to the main shock aftershock type.

关键词

乌什MS7.1地震/余震序列/空间分布/参数分析

Key words

Wushi MS7.1 earthquake/Aftershock sequence/Spatial distribution/Parameter analy-sis

引用本文复制引用

出版年

2024
内陆地震
新疆维吾尔自治区地震局

内陆地震

影响因子:0.495
ISSN:1001-8956
段落导航相关论文